Rock Identifier
Rose Quartz (Silicon dioxide (SiO2) with trace amounts of titanium, iron, or manganese) — mineral
mineral

Rose Quartz

Silicon dioxide (SiO2) with trace amounts of titanium, iron, or manganese

Hardness: 7 on Mohs scale; Color: pale pink to rose red; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Hardness
7 on Mohs scale
Color
pale pink to rose red
Luster
Vitreous (glassy)
Identified More mineral

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Physical properties

Hardness: 7 on Mohs scale; Color: pale pink to rose red; Luster: Vitreous (glassy); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Formation & geological history

Formed in igneous environments, primarily within hydrothermal veins and granitic pegmatites. The pink color is attributed to microscopic inclusions of a fibrous pink mineral similar to dumortierite.

Uses & applications

Used widely in lapidary for jewelry (cabochons, beads), decorative carvings, spheres, figurines, and as a popular specimen for gemstone collectors.

Geological facts

Rose quartz is rarely found as individual crystals and usually occurs as massive chunks. Large deposits found in Brazil and Madagascar can produce boulders weighing several tons.

Field identification & locations

Identify by its distinctive pink color and lack of cleavage. Look for 'milky' or translucent appearances. Commonly found in Brazil, South Africa, India, and Madagascar.